日本地球惑星科学連合2019年大会

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[J] 口頭発表

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT44] 空中からの地球計測とモニタリング

2019年5月26日(日) 15:30 〜 17:00 A07 (東京ベイ幕張ホール)

コンビーナ:楠本 成寿(富山大学大学院理工学研究部(都市デザイン学))、小山 崇夫(東京大学地震研究所)、光畑 裕司(独立行政法人 産業技術総合研究所)、大熊 茂雄(産業技術総合研究所地質情報研究部門)、座長:楠本 成寿小山 崇夫(東京大学 地震研究所 火山センター)、大熊 茂雄(産業技術総合研究所)、光畑 裕司(国立研究開発法人 産業技術総合研究所)

16:15 〜 16:30

[STT44-04] Study of UAV photogrammetry toward efficiently grasping volcanic landform

*岩佐 優一1松島 健2 (1.九州大学大学院理学府地球惑星科学専攻、2.九州大学大学院理学研究院附属地震火山観測研究センター)

キーワード:ドローン、写真測量、火山

In this study, we conducted three-dimensional modeling of volcanic landform using photogrammetry by UAV aerial photography with the aim of efficiently grasp landform. This method, which has been spread in recent years, can grasp landform as not points but planes, and it is thought that this observation can be conducted inexpensively, quickly, and without high-risks. In this study, aiming to make UAV observation efficient, we investigated relation between some factors of UAV observation and the accuracy of 3D model created.

We conducted mission flight on March and August 2018 at Kirishima Iwo-yama located Ebino city, Miyazaki prefecture. Iwo-yama erupted on April 2018, and landform change has occurred. We were able to get photogrammetric data before and after eruption. The UAV used on this study is DJI Mavic pro. The flying altitude from take-off point was 50 m, and the resolution of the images was 1.5 cm/pix. The photographed area was about 0.26 km2, and we set frontlap: the overlap of image along flight route, to 90 %, and sidelap: the overlap of image between flight routes, to 60 %. The UAV flew 60 minutes, and we got 1379 images during each flight. In addition, we measured 16 points as Check points and Ground Control Points (GCP): the points used as standard of coordinates, by GNSS and Total station.

Using Agisoft’s software Photoscan, we created a three-dimensional model before and after eruption from images taken. By increasing a number of measured points, we got more accurate model than that of similar observation in 2017, On the other hand, there were partial vacancy on the model after eruption. This is probably because image processing was not successful due to a lot of volcanic gasses in the photographed image. For solving this problem, at next observation, we photograph from oblique angle in addition to vertical angle only around fumarole.

According to the above data, comparing models, we grasp volcanic landform change due to eruption on April 2018. Furthermore, we investigate relation between particularly GCP and the accuracy of 3D model in order to make UAV observation efficient.

This work was partly supported by MEXT under Integrated Program for Next Generation Volcano Research and Human Resource Development, and under Earthquake and Volcano Hazards Observation and Research Program. Also it was supported by ERI, The University of Tokyo under Joint Usage Program.